Abstract

In this study, aridity data and tree ring data were collected in Northern Serbia, in Southeast (SE) Banat, a subregion within Vojvodina, and Vojvodina at large. They were each investigated independently. The De Martonne Aridity Index and the Forestry Aridity Index are derived from examining the relationship between precipitation and surface air temperature data sets sourced from seven meteorological stations in SE Banat, and from 10 meteorological stations located in Vojvodina as a whole. Vojvodina is a large territory and used as the control area, for the period 1949–2017. The Palmer Drought Severity Index was derived for the period 1927–2016, for both SE Banat and the totality of Vojvodina. The results of the Tree Ring Width Index were obtained from samples collected in or around the villages of Vlajkovac and Šušara, both located in SE Banat, for the period 1927–2017. These tree ring records were compared with three previous aridity and drought indices, and the meteorological data on the surface air temperature and the precipitation, with the objective being to evaluate the response of tree growth to climate dynamics in the SE Banat subregion. It was noted that the significant positive temperature trends recorded in both areas were too insufficient to trigger any trends in aridity or the Tree Ring Width Index, as neither displayed any change. Instead, it appears that these climatic parameters only changed in response to the precipitation trend, which remained unchanged during the investigated period, rather than in response to the temperature trend. It appears that the forest vegetation in the investigated areas was not affected significantly by climate change in response to the dominant temperature increase.

Highlights

  • In recent decades, the issues of climate variability and/or climate change have been the focus of many scientific studies

  • We examine the relationship between tree ring width and local climatic parameters, in order to evaluate the efficacy of the Tree Ring Width Index (TRWI) in evaluating the aridity

  • It appears that the change in aridity/drought trends cannot be the result of only a change in temperature trends

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Summary

Introduction

The issues of climate variability and/or climate change have been the focus of many scientific studies. Global climate change, caused by natural processes as well as anthropogenic factors, is a major environmental issue that may have a significant impact on the world over the course of the 21st century [1,2,3,4]. Governments, the scientific community, the media, and people all over the world have been paying more and more attention to recent trends in global climate change [5]. Temperature change [6], precipitation change [7] and the rate of these changes are some of the most important drivers of climate change. It seems to be more useful to analyze temperature and precipitation simultaneously, which is most similar to their impact on climate.

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